Abstract
IN connexion with a study of the reaction mechanism of the thermal decomposition of dolomite, we are investigating exchange between carbon-13 dioxide (13CO2) and solid carbonates at high temperatures. To our knowledge exchange reactions using isotopic tracers between gaseous and solid reactants have, so far, only been carried out1,2 on oxides and oxygen-18.
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References
Allen, J. A., and Lauder, I., Nature, 164, 142 (1949).
Houghton, G., and Winter, E. R. S., Nature, 164, 1130 (1949).
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HAUL, R., STEIN, L. & LOUW, J. Exchange of Carbon-13 Dioxide between Solid Carbonates and Gaseous Carbon Dioxide. Nature 167, 241–242 (1951). https://doi.org/10.1038/167241b0
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DOI: https://doi.org/10.1038/167241b0
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